Fluorite CaF2 70%

Fluorite, chemically calcium fluoride (CaF₂), is a typical halide mineral and the primary global feedstock for fluorine supply across fluorochemical, metallurgical, glass and ceramic industries. It forms endogenously from magmatic hydrothermal activity. During magma cooling, magma-separated hydrothermal fluids are rich in fluoride constituents. As these fluids migrate upward through rock fractures, gradual drops in temperature and pressure trigger a chemical reaction:

Spate fluorurata metallurgica mongola con CaF₂ ≥70%, che fornisce un flusso affidabile per la produzione dell'acciaio. Presenta composizione stabile, basse impurità e fornitura flessibile, garantendo qualità costante e consegna globale affidabile.